江西鹰潭月湖岩大型石拱地质特征及成因分析

邓宗裕, 陈留勤, 杨柳, 刘鑫. 2024. 江西鹰潭月湖岩大型石拱地质特征及成因分析. 华东地质, 45(4): 478-487. doi: 10.16788/j.hddz.32-1865/P.2023.12.016
引用本文: 邓宗裕, 陈留勤, 杨柳, 刘鑫. 2024. 江西鹰潭月湖岩大型石拱地质特征及成因分析. 华东地质, 45(4): 478-487. doi: 10.16788/j.hddz.32-1865/P.2023.12.016
DENG Zongyu, CHEN Liuqin, YANG Liu, LIU Xin. 2024. Geological characteristics and genesis of the large rock arch at Yuehuyan in Yingtan City of Jiangxi Province. East China Geology, 45(4): 478-487. doi: 10.16788/j.hddz.32-1865/P.2023.12.016
Citation: DENG Zongyu, CHEN Liuqin, YANG Liu, LIU Xin. 2024. Geological characteristics and genesis of the large rock arch at Yuehuyan in Yingtan City of Jiangxi Province. East China Geology, 45(4): 478-487. doi: 10.16788/j.hddz.32-1865/P.2023.12.016

江西鹰潭月湖岩大型石拱地质特征及成因分析

  • 基金项目: 国家自然科学基金“中国东南和西北地区丹霞地貌陡坡上洞穴成因对比研究(编号:42361002)”项目资助。
详细信息
    作者简介: 邓宗裕,2000年生,女,硕士研究生,主要从事丹霞地貌研究工作。Email:1973270747@qq.com
    通讯作者: 陈留勤,1983年生,男,教授,博士,主要从事沉积岩、丹霞地貌与旅游地学研究工作。Email:liuqincheen@163.com
  • 中图分类号: P931

Geological characteristics and genesis of the large rock arch at Yuehuyan in Yingtan City of Jiangxi Province

More Information
  • 石拱是丹霞地貌区重要的景观要素之一,大者又被称为天生桥,具有重要的地貌学研究意义和旅游开发价值。月湖岩大型石拱位于江西信江盆地西部,是我国湿润区石拱的典型代表,目前对其成因鲜有报道。文章通过野外地质调查、水分测试及室内样品薄片显微观察和盐化学实验,研究月湖岩大型石拱的地质特征并探讨其成因。结果表明:研究区NNE向和近EW向断裂控制了石拱的空间产状;石拱由晚白垩世塘边组风成砂岩组成,地层产状平缓,发育大型交错层理,结构成熟度高,渗透性较好,但成分成熟度低,富含化学稳定性较弱的长石、岩屑及钙质胶结物,有利于发生溶蚀风化;断裂和层理交汇处的岩石较破碎,在河流侵蚀作用下易发生溶蚀,风化物质随流水从山体底部流出,随着溶蚀和崩塌的持续发生,研究区山体南、北两侧被侵蚀穿透,最终形成石拱。文章为理解丹霞地貌区石拱的成因机制提供了实际材料,同时对石拱保护和旅游开发具有参考价值。

  • 加载中
  • 图 1  研究区位置图

    Figure 1. 

    图 2  鹰潭市1960—2020年气候参数变化图

    Figure 2. 

    图 3  月湖岩石拱景观及地貌特征

    Figure 3. 

    图 4  月湖岩石拱垂直方向相对湿度变化图

    Figure 4. 

    图 5  月湖岩砂岩显微照片及粒度分析图

    Figure 5. 

    图 6  月湖岩石拱演化过程图

    Figure 6. 

    表 1  月湖岩样品电导率与盐化学实验结果

    Table 1.  Conductivity and salt chemistry results of samples at Yuehuyan

    样品编号 电导率 K+ Na+ Ca2+ Mg2+ Cl SO42− NO3
    μS/cm mg/L
    YHY-22-1 155.0 2.70 0.80 12.3 0.80 7.30 5.90 1.00
    YHY-22-2 1670.0 11.0 3.60 165 9.70 40.1 317 434
    YHY-22-3 2090.0 10.2 8.10 237 13.5 54.7 362 675
    YHY-22-4 1280.0 7.30 4.30 108 11.2 36.5 53.2 608
    YHY-22-5 1290.0 8.50 2.50 159 6.70 7.30 399 47.9
    下载: 导出CSV
  • [1]

    BRUTHANS J, SOUKUP J, VACULIKOVA J, FILIPPI M, SCHWEIGSTILLOVA J, MAYO A L, MASIN D, KLETETSCHKA G, RIHOSEK J. 2014. Sandstone landforms shaped by negative feedback between stress and erosion[J]. Nature Geoscience,7(8):597-601. doi: 10.1038/ngeo2209

    [2]

    CHEN X, CHEN L Q, ZHANG Y H, DU D D, HU H P, LIU D X, LI W Z. 2021. Lithological and environmental controls on large tafoni along conglomerate cliffs in subtropic humid Danxiashan UNESCO Global Geopark[J]. Journal of Mountain Science,18(5):1131-1143. doi: 10.1007/s11629-020-6649-3

    [3]

    CHEN L Q, GUO F S, LIU F J, XU H, DING T, LIU X. 2019. Origin of tafoni in the Late Cretaceous aeolian sandstones, Danxiashan UNESCO Global Geopark, South China[J]. Acta Geologica Sinica-English Edition,93(2):451-463. doi: 10.1111/1755-6724.13810

    [4]

    CHEN L Q, GUO F S, SHAO C J, DU D D, CHEN F, LUO M. 2022. Geodiversity characterization of the Danxiashan UNESCO Global Geopark of China[J]. International Journal of Geoheritage and Parks,10(4):459-476. doi: 10.1016/j.ijgeop.2022.07.003

    [5]

    CHEN L Q, GUO F S, SHAO C J, LOU F S, LI B, LI G R, QIE H M, WU Z Y, JIANG Y B, LIU F J. 2022. Characteristics and controlling factors of Danxia landscapes in Jiangxi Province[J]. Acta Geologica Sinica,96(11):4023-4037 (in Chinese with English abstract).

    [6]

    GOUDIE A S. 2016. Quantification of rock control in geomorphology[J]. Earth-Science Reviews,159:374-387. doi: 10.1016/j.earscirev.2016.06.012

    [7]

    GUO F S, CHEN L Q, YAN Z B, LIU F J, PAN Z X, ZHANG W Q, HU H P. 2020. Definition, classification, and danxianization of Danxia landscapes[J]. Acta Geologica Sinica,94(2):361-374 (in Chinese with English abstract).

    [8]

    GUO F S, LING Y Y, CHEN L Q, ZHOU W P, LI H W, CHENG L K, WU Z C, LI G R, GUO Z, LI B. 2023. Controlling factors and types of geomorphologic landscapes in Danxiashan UNESCO Global Geopark of China[J]. Geoscience,37(6):1665-1679 (in Chinese with English abstract).

    [9]

    HUANG L Q, WU C H, ZHOU L Y, JIN N, PENG S L, HU N Y, YANG C M, CHEN J. 2023. New perspectives of the features, formation, and evolution of the special Danxia landscape in Chenzhou, Hunan[J]. Geoscience,37(6):1680-1694 (in Chinese with English abstract).

    [10]

    JIANG Y B, GUO F S, CHEN S S. 2013. Spatial distribution and its genesis of the Danxia landforms in Xinjiang basin, Jiangxi[J]. Mountain Research,31(6):731-737 (in Chinese with English abstract).

    [11]

    JIANG F W, GUO F S, YANG A L. 2018. Differential expansion and contraction characteristics of Danxia landform rock mass and its geomorphological effect[J]. Mountain Research,36(4):501-508 (in Chinese with English abstract).

    [12]

    LI X N, JIANG Y B, WANG P P. 2023. Features and genesis analysis of Danxia landscape in the northwest foothills of the Wuyi Mountains[J]. East China Geology,44(2):228-238 (in Chinese with English abstract).

    [13]

    LIU D X, CHEN X, CHEN L Q, GUO F S, LIU F J. 2022. Genesis of tafoni in the Cuiwei Peak, Jiangxi province, China[J]. Mountain Research,40(2):196-204 (in Chinese with English abstract).

    [14]

    LIU X, GUO F S, CHEN L Q, LI X M, LIU F J. 2019. Lithologic control on the development of Danxia landscapes in red basins[J]. Mountain Research,37(2):214-221 (in Chinese with English abstract).

    [15]

    LU F, ZHANG Y, ZHANG X H, MO Z F, LÜ J S, WU B. 2023. Zircon U-Pb geochronology, geochemical characteristics and geological significance of the Chakeng granite porphyry, northeast Jiangxi Province[J]. East China Geology,44(1):39-50 (in Chinese with English abstract).

    [16]

    OSTANIN I, SAFONOV A, OSELEDETS I. 2017. Natural erosion of sandstone as shape Optimisation[J]. Scientific Reports,7(1-4):17301.

    [17]

    PENG X H, WU H, LI X W, ZHANG Y, ZHU J. 2021. Danxia landform types and development mechanism in Yan’an City[J]. Arid Land Geography,44(2):418-426 (in Chinese with English abstract).

    [18]

    RIHOSEK J, BRUTHANS J, MASIN D, FILIPPI M, CARLING G T, SCHWEIGSTILLOVA J. 2016. Gravity-induced stress as a factor reducing decay of sandstone monuments in Petra, Jordan[J]. Journal of Cultural Heritage,19:415-425. doi: 10.1016/j.culher.2015.10.004

    [19]

    ŘIHOŠEK J, SLAVÍK M, BRUTHANS J, FILIPPI M. 2019. Evolution of natural rock arches: a realistic small-scale experiment[J]. Geology,47(1):71-74. doi: 10.1130/G45421.1

    [20]

    SHI Y X, CHEN L Q, DU D D, CHAI L, WANG Z H. 2023. Basic characteristics and genesis of cavernous weathering features on the steep slopes of Danxia landscape in Danxiashan UNESCO Global Geopark[J]. Tropical Geography,43(1):103-114 (in Chinese with English abstract).

    [21]

    STARR A M, MOORE J R, THORNE M S. 2015. Ambient resonance of mesa arch, Canyonlands National Park, Utah[J]. Geophysical Research Letters,42(16):6696-6702. doi: 10.1002/2015GL064917

    [22]

    TAN Y F, LI L H, HUANG B X. 2021. Contrasting characteristics and origin of Danxia arched rock shelters in Zhejiang, China, and natural arches and bridges on the Colorado Plateau, USA[J]. Journal of Geographical Sciences,31(6):802-818. doi: 10.1007/s11442-021-1872-6

    [23]

    TAN Y F, LI L H, YANG Z F, LIAO X H. 2019. Moisture stress effect and its control on differential weathering of red-bed sandstone and conglomerate[J]. Chinese Journal of Rock Mechanics and Engineering,38(S2):3481-3492 (in Chinese with English abstract).

    [24]

    TAN Y, ZHU C, WU L, SUN W, WANG X C, JIA T J, PENG H, HOU R F. 2015. Geomophogensis on sandstone honeycombs and white spot in the Mt. Danxiashan, Guangdong Province, South China[J]. Mountain Research,33(3):279-287 (in Chinese with English abstract).

    [25]

    WANG Y J, CHEN L Q, LI W H, LI P C. 2019. Detrital zircon U-Pb dating of the Late Cretaceous aeolian sandstones from the Tangbian Formation in the Yiyang area of Jiangxi Province and its provenance significance[J]. Geological Bulletin of China,38(4):667-679 (in Chinese with English abstract).

    [26]

    WANG G L, LIANG Z Y, ZHANG L, SUN F. 2018. Study of influence mechanism of Z-type fissure on sandstone strength and fracture behavior[J]. Rock and Soil Mechanics,39(S2):389-397 (in Chinese with English abstract).

    [27]

    WANG Y, WANG Y J, LI S B, SEAGREN E, ZHANG Y Z, ZHANG P Z, QIAN X. 2020. Exhumation and landscape evolution in eastern South China since the Cretaceous: new insights from fission-track thermochronology[J]. Journal of Asian Earth Sciences,191:104239. doi: 10.1016/j.jseaes.2020.104239

    [28]

    WU Z J, QIU L W, WANG H P, ZHONG M S, GAO F L, HOU J, LI X. 2023. Discovery and significance of salt weathering tafoni in Meso-Neoproterozoic sandstone in Dalian area, Liaoning Province[J]. Geological Review,69(6):2158-2160 (in Chinese with English abstract).

    [29]

    YANG H K. 2017. Genesis on the characteristics and formation mechanism of the Danxia landform in Zhejiang Province Jiangxi Province and Fujian Province [D]. Nanjing: Nanjing University (in Chinese with English abstract).

    [30]

    YANG M G, WANG G H, XU M G, HU Q H. 2016. Basic characteristics of the Marina Pacific tectonic activities in Jiangxi Province and its adjacent areas[J]. East China Geology,37(1):10-18 (in Chinese with English abstract).

    [31]

    ZHAO K, RAN S H, ZENG P, YANG D X, TENG T Y. 2021. Effect of moisture content on characteristic stress and acoustic emission characteristics of red sandstone[J]. Rock and Soil Mechanics,42(4):899-908 (in Chinese with English abstract).

    [32]

    ZHU C, PENG H, LI S C, HUANG L Y, ZHENG C G, XIANG F S, SUN Y F, TANG Y S, HU J Y, ZHU G H, LU J J, CHENG G H. 2005. Danxia landform genesis on Qiyun Mountain, Anhui Province[J]. Acta Geographica Sinica,60(3):445-455 (in Chinese with English abstract).

    [33]

    陈留勤, 郭福生, 邵崇建, 楼法生, 李斌, 黎广荣, 郄海满, 吴知勇, 姜勇彪, 刘富军. 2022. 江西省丹霞地貌特征及其控制因素探讨[J]. 地质学报,96(11):4023-4037. doi: 10.3969/j.issn.0001-5717.2022.11.024

    [34]

    郭福生, 陈留勤, 严兆彬, 刘富军, 潘志新, 张炜强, 胡海平. 2020. 丹霞地貌定义、分类及丹霞作用研究[J]. 地质学报,94(2):361-374. doi: 10.3969/j.issn.0001-5717.2020.02.002

    [35]

    郭福生, 凌媛媛, 陈留勤, 周万蓬, 李宏卫, 程亮开, 吴志春, 黎广荣, 国振, 李斌. 2023. 丹霞山世界地质公园地貌景观控制因素与景观类型研究[J]. 现代地质,37(6):1665-1679.

    [36]

    黄乐清, 吴驰华, 周丽芸, 金妮, 彭世良, 胡能勇, 杨长明, 陈杰. 2023. 湖南郴州丹霞地貌景观特征、成因及演化探讨[J]. 现代地质,37(6):1680-1694.

    [37]

    姜勇彪, 郭福生, 陈珊珊. 2013. 江西信江盆地丹霞地貌空间分布及其成因[J]. 山地学报,31(6):731-737. doi: 10.3969/j.issn.1008-2786.2013.06.012

    [38]

    姜伏伟, 郭福生, 杨安林. 2018. 丹霞地貌岩体差异胀缩特征及其成景作用[J]. 山地学报,36(4):501-508.

    [39]

    李晓宁, 姜勇彪, 王盼盼. 2023. 武夷山脉西北麓丹霞地貌特征及成因分析[J]. 华东地质,44(2):228-238.

    [40]

    刘东兴, 陈欣, 陈留勤, 郭福生, 刘富军. 2022. 江西宁都翠微峰蜂窝状洞穴特征及成因[J]. 山地学报,40(2):196-204.

    [41]

    刘鑫, 郭福生, 陈留勤, 李馨敏, 刘富军. 2019. 红层盆地岩性差异对丹霞地貌发育的控制[J]. 山地学报,37(2):214-221.

    [42]

    陆凡, 张勇, 张雪辉, 莫子奋, 吕劲松, 武彬. 2023. 赣东北茶坑花岗斑岩锆石U-Pb年代学、地球化学特征及地质意义[J]. 华东地质,44(1):39-50.

    [43]

    彭小华, 吴昊, 李兴文, 张瑜, 祝捷. 2021. 延安地区丹霞地貌类型及发育机制研究[J]. 干旱区地理,44(2):418-426. doi: 10.12118/j.issn.10006060.2021.02.13

    [44]

    史月欣, 陈留勤, 杜丁丁, 柴乐, 王子涵. 2023. 丹霞山陡坡上风化洞穴的基本特征及成因探讨[J]. 热带地理,43(1):103-114.

    [45]

    谭玉芳, 李丽慧, 杨志法, 廖小辉. 2019. 红层砂岩与砾岩差异风化的湿度应力效应研究[J]. 岩石力学与工程学报,38(S2):3481-3492.

    [46]

    谭艳, 朱诚, 吴立, 孙伟, 王晓翠, 贾天骄, 彭华, 侯荣丰. 2015. 广东丹霞山砂岩蜂窝状洞穴及白斑成因[J]. 山地学报,33(3):279-287.

    [47]

    王宇佳, 陈留勤, 李文灏, 李鹏程. 2019. 江西弋阳晚白垩世塘边组风成砂岩碎屑锆石U-Pb定年及其物源意义[J]. 地质通报,38(4):667-679.

    [48]

    王桂林, 梁再勇, 张亮, 孙帆. 2018. Z型裂隙对砂岩强度和破裂行为影响机制研究[J]. 岩土力学,39(S2):389-397.

    [49]

    吴子杰, 邱隆伟, 王海鹏, 仲米山, 高福亮, 侯静, 李欣. 2023. 辽宁大连地区中—新元古界砂岩盐风化穴的发现及意义[J]. 地质论评,69(6):2158-2160.

    [50]

    杨昊坤. 2017. 浙赣闽典型丹霞地貌景观特征与形成机理[D]. 南京: 南京大学.

    [51]

    杨明桂, 王光辉, 徐梅桂, 胡青华. 2016. 江西省及邻区滨太平洋构造活动的基本特征[J]. 华东地质,37(1):10-18.

    [52]

    赵奎, 冉珊瑚, 曾鹏, 杨道学, 腾天野. 2021. 含水率对红砂岩特征应力及声发射特性的影响[J]. 岩土力学,42(4):899-908.

    [53]

    朱诚, 彭华, 李世成, 黄林燕, 郑朝贵, 项伏生, 孙毓飞, 唐云松, 胡济源, 朱光辉, 吕健君, 程光华. 2005. 安徽齐云山丹霞地貌成因[J]. 地理学报,60(3):445-455.

  • 加载中

(6)

(1)

计量
  • 文章访问数:  166
  • PDF下载数:  27
  • 施引文献:  0
出版历程
收稿日期:  2023-12-27
修回日期:  2024-06-17
录用日期:  2024-05-27
刊出日期:  2024-12-28

目录